Mammals of Washington, Volume 2: University of Kansas Publications Museum of Natural HistoryDalquest, Walter Woelber
Science
Mammals of Washington, Volume 2: University of Kansas Publications Museum of Natural History
Dalquest, Walter Woelber
Mammals -- Washington (State)
The part of eastern Washington south of the Okanogan Highland Province,
save the extreme southeastern corner of the state, constitutes the
Columbia Lava Province. This is an extensive, relatively level plateau
that lies mainly below 2,000 feet elevation. The plateau consists of
gently folded lava flows that reach a depth of 4,000 feet in some
places (Russell, 1893) and slope inward from the east, north, and,
in part, the west (Flint, 1938). These horizontal layers of basalt
are extremely resistant to erosion by other than large rivers. Two
great gashes cross the Plateau diagonally from the northeast to the
southwest; these are Moses Coulee and the Grand Coulee. These old
coulees are the former valleys of the Columbia River, and were formed
at the time when the course of the river was successively blocked by
the advance of Pleistocene ice. The Snake River crosses the southern
edge of the Columbia Lava Province and separates the plateau proper
from an area of similar land to the southward.
[Illustration: FIG. 2. Columbia River one mile west of Kellers Ferry,
Washington, elevation 1,060 feet, April 16, 1940. (Fish and Wildlife
Service photo by Victor B. Scheffer, No. 933.)]
The Blue Mountains Province is an area of relatively small extent in
the extreme southeastern corner of the state of Washington. There, the
province concerned constitutes, as it were, a northward extension of
the Blue Mountains of Oregon. The mountains rise to only 5,000 feet
elevation in the Washington part of the Blue Mountains Province.
DISTRIBUTIONAL AREAS
The physiographic provinces are areas of land form. The form of the
land has a considerable effect on the temperature, humidity, drainage,
weathering, soil, and other non-organic features that combine to
produce the various life-zones and influence the distribution of
mammals. One might therefore expect a close correlation of mammalian
distributional areas with physiographic provinces. Although there is
a correlation, it is not exact because the distribution of mammals is
influenced also by certain other factors. Among these are historical
factors and isolation by geographic barriers.
[Illustration: FIG. 3. Mammalian distributional areas of Washington.
A. Western Washington. B. Cascade Mountains. C. Northeastern
Washington. D. Blue Mountains. E. Southeastern Washington.
F. Yakima Valley. G. Columbian Plateau.]
The Cascade Mountains Province of Culver includes the Yakima Valley
Area. This province contains two completely different mammalian
distributional areas. The higher mountains possess a boreal, alpine
fauna; the Cascade Range itself is called the Cascade Area in this
report. The Yakima Valley Area possesses a desert fauna derived from
the desert of eastern Oregon.
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